Guide HIKING/VANDRE LYNGENFJORD
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Tromsø - Winter Auroras & Crystal Lavvos Glamping
Viewed: 29 Sep 2021 Tromsø - Winter Auroras & Crystal Lavvos Glamping HOLIDAY TYPE: Flexible Dates BROCHURE CODE: 26029 VISITING: Norway DURATION: 3 nights In Brief This three-night trip is an ideal mix of winter adventure and cultural city exploration. Go from discovering the bustling city of Tromsø to snowmobiling in the Lyngen Alps before retiring to your glass-roofed Crystal Lavvo for all-night Aurora opportunities. Speak to us on 01670 785 012 [email protected] www.theaurorazone.com PAGE 2 What's included? ALL OF THE ACTIVITIES AND SERVICES LISTED BELOW ARE INCLUDED IN THE HOLIDAY PRICE • Transfers: return airport transfers • Accommodation: 2 nights at Clarion Hotel The Edge in a standard twin/double room and 1 night in a Crystal Lavvo • Meals: 3 breakfasts, 1 lunch, 1 dinner and 1 light dinner • The following activities are included in the holiday price: snowmobile safari, overnight in a Crystal Lavvo, visit to the husky centre and Aurora Camp (order subject to change) • Cold weather clothing during activities • Fully qualified guides and instructors during activities Trip Overview As the largest city in Northern Norway and sitting 350 kilometres north of the Arctic Circle, Tromsø is the perfect combination of natural wonders and vibrant city life. Nicknamed ‘the gateway to the Arctic’ and renowned for its Northern Lights potential, Tromsø gives you easy access to some truly wonderful winter experiences both day and night, which we make the most of during this itinerary. You will spend some time outside of the city centre and in the stunning Lyngen Peninsula where you will explore the breathtaking scenery by snowmobile before retiring to your dedicated Aurora accommodation. -
The Story of MIT-Fablab Norway: Community Embedding of Peer Production
Journal of Peer Production ISSN: 2213-5316 http://peerproduction.net The Story of MIT-Fablab Norway: Community Embedding of Peer Production Cindy Kohtala and Camille Bosqué Abstract: MIT-Fablab Norway was one of the first Fab Labs ever established, in northern Norway in 2002. Despite this auspicious beginning to a network that is rapidly growing, surprisingly little has been written about the genesis of the network or the Fab Lab itself. We therefore aim to contribute to this knowledge gap with a narrative account of our independent ethnographic research visits to the Lab. We combine our researcher perspectives, which are informed by, on the one hand, Aesthetics and a phenomenological understanding and, on the other, Science and Technology Studies, with Design Research bridging both. Our account aims to richly describe the Lab’s unique profile in the MIT Fab Lab network as a socially shaped entity and product of a particular time and place. Most salient in this narrative is the role of its charismatic founder, whose stories and metaphors become vehicles by which we come to understand how a Fab Lab forms its own identity, balancing the relationships with local stakeholders against those with the Fab Lab network; how it promotes certain principles and values of peer production; and how it represents itself to both maker insiders and outsiders. While situated and particular to this Lab, our interpretations may have implications for the trajectories of other Fab Labs and makerspaces, as well as our understanding of peer production as a new paradigm. Keywords: Fab Lab, ethnography, MIT-Fablab Norway, material peer production Cindy Kohtala and Camille Bosqué In spite of this emerging body of work, there remains a certain mystique that surrounds Fab Labs, their objectives and activities. -
Laser Measurement of Pave- Ment Condition E8 Borealis, Skibotn – Border Finland
Drift og vedlikehold Laboratorier og grunnboring Laboratorium midt 20.05.2021 Laser measurement of pave- ment condition E8 Borealis, Skibotn – Border Finland STATENS VEGVESENS RAPPORTER Nr. 712 Statens vegvesen Statens NPRA reports Statens vegvesens rapporter Norwegian Public Roads Administration Tittel Title Dekketilstandsmålinger med laser på E8 Laser measurement of pavement condition Borealis – Spor, jevnhet, tverrfall og MPD on E8 Borealis Undertittel Subtitle E8 Borealis, Skibotn – Riksgrense Finland, E8 Borealis, Skibotn – Border Finland Troms- og Finnmark fylke Forfatter Author Trond Østen Trond Østen Avdeling Department Laboratorier og grunnboring Laboratories and Soil Boring Seksjon Section Laboratorium midt Laboratory Central Norway Prosjektnummer Project number C13404 C13404 Rapportnummer Report number Nr. 712 No. 712 Prosjektleder Project manager Leif Jørgen Bakløkk Leif Jørgen Bakløkk Godkjent av Approved by Doreen Siebert Doreen Siebert Emneord Key words IRI, spor, tekstur og lasermåling IRI, ruts, textur and laser measurement Sammendrag Summary I forbindelse med testprosjektet E8 Borealis i In 2019, the Directorate of Public Roads in 2019 ønsket Statens vegvesen å sammenligne the Norwegian Public Roads Administration ulike utstyr for måling av dekketilstand og (NPRA) aimed to compare various equipt- få dokumentasjon på forskjeller og fordeler/ ment’s for measuring pavement condition and ulemper for de ulike systemer. I tillegg er det get documentation of the different systems. ønskelig å få best mulig dokumentasjon av In addition, the NPRA was seeking the best dekketilstand på E8 Skibotn – Riksgrense possible documentation of pavement condi- Finland i Troms og Finnmark fylke. Målingene tion on the E8 test road, both with regard to er gjort både med tanke på overflatetilstand surface condition (ruts, evenness, damage, (spor, jevnhet, skader, tekstur og friksjon) og texture, etc) and the structural strength/ strukturell styrke/bæreevne og vegen opp- load-bearing capacity, as well as pavement bygging. -
Lyngen Alps in the Arctic Circle Is an Expedition of a Lifetime
Norwegian Skiing summit to sea amongst the serenity and astounding beauty of Norway’s Lyngen Alps in the Arctic Circle is an expedition of a lifetime CONQUEST + BY JULIE NIEUWENHUYS PHOTOGRAPHS BY CAROLINE VAN ’t HOFF 26 S–Magazine SNOWSPORTSCULTURE.COM SNOWSPORTSCULTURE.COM S–Magazine 27 BLUE SKIES, SCREECHING SEAGULLS AND SALTY SEA AIR; for a fleeting moment I wonder if I’m in the Mediterranean. But then reality hits me when I jump into the deep blue water off the sailboat, the Arctic Ice and shock sets in. It might have been brash to jump off a snowy boat into an ice-cold fjord so I quickly put on some clothes and am handed a typical Norse specialty; a shot of Aquavit, a double distilled potato 40% liqueur.. Skål! While most skiers stored away their skis in April, it is not quite the end of our winter. We found the ultimate way to prolong our ski season by a few weeks. We are at the small Norwegian airport of Tromsø, 300 kilometres above the Arctic Circle, where we welcome our tired friends, who have flown in from North America. Our crew for this Arctic adventure consists of pro skier Molly Baker, a film crew from Mt. Baker and a few of our lucky Dutch friends. It’s an eclectic group and although our backgrounds are completely different, we all share a passion for skiing. For the next month we’ll be traveling by ski, boat and car through the Lyngen Alps in Northern Norway. In this remote area on the same latitude as Siberia and Alaska, where impressive mountains and deep blue fjords dominate the scenery. -
ASTARTE Test Site Lyngen Carl B
ASTARTE test site Lyngen Carl B. Harbitz NGI ASTARTE WP9 Meeting Paris, 23-24 January 2014 Lyngen test site, northern Norway • Potential rockslide from the mountain Nordnes, 7 km from the village Lyngseidet • Volume estimate up to 22 Mm3 with 11 Mm3 as the most likely upper limit 1810 Rock slide tsunami from Pollfjellet Mountain Among the largest rock slides in Norway 2 km wide head scar, 20 km south of Nordnes Waves observed more than 20 km away in both directions 3 large waves 2 m high waves in the head of the fjord 14 perished, large damages Today: Road tunnel to protect snow avalanches and rockfalls Submarine landslide tsunami sources (1) • At least 6 very large landslides have occurred in the Norwegian and Greenland Basins during the last ~20ka, giving a frequency of 1 in ~3-to-4000 years • The 8200 BP Storegga Slide produced a far field tsunami • This project will consider tsunamis generated at 3 different locations within the Norwegian and Greenland Basins to capture the effects of variable source location Submarine landslide tsunami sources (2) • Modelling will consider a range of landslide motions, including how multi-stage failure affects tsunami generation • Slide motion will be informed by field studies of the Trænadjupet Slide, which is the last major slide at ~4 ka. • This work will extend from a £2.3 Million UK (NERC) funded research project, which includes a 1 month research cruise to map and date the Trænadjupet Slide in summer 2014 What has already been done by NGI? • 3 reports on rockslide tsunamis in Lyngen • 2008, 2010, 2013 • Updated volume estimates • Refined inundation modelling • NGI’s results are the official ones used by the local authorities for evacuation and land-use planning, etc. -
TOUR OPERATOR MANUAL 20/21 Northern Lights Season
TOUR OPERATOR MANUAL 20/21 Northern Lights season THE UNDISCOVERED ARCTIC Lyngen is a truly unique and magical Our beautiful location still has its destination - we can’t wait to share it authenticity though, and the “true feel” with you! of rural Northern-Norway. With a rich heritage, culture & colourful language, Situated on a small peninsula we are definitely a location of choice. surrounded by alpine mountains and fjords in every direction, we have Combine this with spectacular scenery, historically been somewhat isolated. un-spoilt nature, and the most Thanks to our ferry system, we are now welcoming locals you could imagine! even more accessible than ever - just an 87-minute drive from Tromsø by car. We look forward to welcoming you on your next adventure. Lyngen is still undeveloped in terms of tourism but make no mistake, we have a lot to offer! Sarah Burrows – Manager TABLE OF CONTENTS Activity Descriptions Arctic Whisky Experience 4 Snowmobile Safari 5 Dog-Sledding 6 Northern Lights Evening 7 Whale Safari 8 Accommodation Options Aurora Fjord Cabins 9 Sørheim Brygge 10 Booking Info 11 Price Lists Activities 12 Accommodation 14 Arctic Whisky Experience An Exciting Day Tour to the Worlds Northern-most Distillery! Aurora Spirit has established the world’s Recommended For: most northerly Distillery. The Lyngen Alps, We recommend this tour especially for those the fjords and the Arctic wilderness are an with an interest in history and tasting. excellent setting for making whisky! At their However, the tour is suitable for most and is a spectacular visitor center, you can take part good and easy introduction to arctic in guided tours with complimentary tasting ingredients and scenery. -
Turen Går Til Steindalen
A TRIP TO STEINDALEN A trip to Steindalen Excursion guide Please take this with you on your trip, - geology and landscape on the way to the glacier but don’t leave it behind as litter. A part of ”Geologiskolen”, http://geologiskolen.uit.no/ Text and photos: Associate professor Geoffrey D. Corner Design: Kjell T. Svindland Department of Geology University of Tromsø NO-9037 Tromsø NORWAY Geoffrey D. Corner Universitety of Tromsø 2008 http://geologiskolen.uit.no/lokalGeologiskolen/storfjord.html Sheet 1 of 9 Overview Practical information The Steindalen glacier (Steindalsbreen) in Lyngen is a popular destination for Steindalen is located on the people who would like to see a glacier at close quarters. The glacier front is eastern side of the Lyngen situated just 460 m a.s.l. and the walk up to it takes no more than a couple of hours. Peninsula, south of Lyngsdalen and Furuflaten. The twelve localities in this excursion guide show places along the way that reveal From Oteren, drive north the landscape history of the area and how the glacier has retreated after the ice age. for c. 17 km on the west The first locality lies at the entrance to the valley; the last one is at the glacier front. side of Storfjorden to just The table below gives an overview. past Storeng. Cross the bridge over Steindalselva and turn left up a steep gravel path between the houses. This path leads to a community house and a small car park. The 1 River terraces 2 Rock treshold 3 Rapids 4 Rockslide walking track up (90 m) (200-250 m) (240 m) moraine (250 m) Steindalen begins here. -
Troms Politidistrikt
Dato 2016-10-10 TROMS POLITIDISTRIKT POLITIMESTERENS HØRING - STRUKTUR TJENESTESTEDER OG TJENESTEENHETER I TROMS POLITIDISTRIKT HØRING INNHOLD 1. SAMMENDRAG ............................................................................................................................ 3 2. INNLEDNING ................................................................................................................................ 4 2.1 BAKGRUNN OG FORMÅL .................................................................................................................... 4 2.2 AVGRENSNINGER OG AVHENGIGHETER ..................................................................................... 6 2.3 TILNÆRMING OG ORGANISERING ................................................................................................. 7 2.3.1 METODE ................................................................................................................................................. 9 2.3.2 BEGREPSAVKLARINGER .............................................................................................................. 10 3. DAGENS SITUASJON ............................................................................................................... 13 3.1 POLITIDISTRIKTETS GEOGRAFI .................................................................................................. 13 3.1.1 TROMS POLITIDISTRIKT ............................................................................................................. 13 3.1.2 TROMS POLITIDISTRIKTS -
Kommunedelplan E6-E8 Skibotn, Storfjord Kommune; Konsekvenser for Dyre Og Fuglelivet
Kommunedelplan E6-E8 Skibotn, Storfjord kommune; konsekvenser for dyre og fuglelivet SteinØ.Nilsen Karl-Birger Strann NINA• NIKU NINA Norsk institutt for naturforskning Kommunedelplan E6-E8 Skibotn, Storfjord kommune; konsekvenser for dyre og fuglelivet Stein Ø. Nilsen Karl-Birger Strann NINA Norsk institutt for natwforskning nina oppdragsmelding 495 Nilsen, S.Ø. & Strann, K-B. 1997 , Kommunedelplan NINA•NIKUs publikasjoner E6-E8 Skibotn, Storfjord kommune; konsekvenser for dyre- og fuglelivet. NINA Oppdragsmelding 495: 1-12 NINA•NIKU utgir følgende faste publikasjoner: Tromsø, september 1997 NINA Fagrapport NIKU Fagrapport ISSN 0802-4103 Her publiseres resultater av NINAs og NIKUs eget fors- ISBN 82-426-0846-6 kningsarbeid, problemoversikter, kartlegging av kunn- skapsnivået innen et emne, og litteraturstudier. Rapporter Forvaltningsområde: utgis også som et alternativ eller et supplement til inter- Naturinngrep nasjonal publisering, der tidsaspekt, materialets art, mål- Management area: gruppe m.m. gjør dette nødvendig. Major land use change Opplag: Normalt 300-500 NINA Oppdragsmelding Rettighetshaver (D: NIKU Oppdragsmelding Stiftelsen for naturforskning og kulturminneforskning Dette er det minimum av rapportering som NINA og NIKU NINA•NIKU gir til oppdragsgiver etter fullført forsknings- eller utred- ningsprosjekt. I tillegg til de emner som dekkes av fag- Publikasjonen kan siteres fritt med kildeangivelse rapportene, vil oppdragsmeldingene også omfatte befar- ingsrapporter, seminar- og konferanseforedrag, års- rapporter fra overvåkningsprogrammer, o.a. Opplaget er begrenset. (Normalt 50-100) Temahefter Disse behandler spesielle tema og utarbeides etter behov Redaksjon: bl.a. for å informere om viktige problemstillinger i Kjell Einar Erikstad samfunnet. Målgruppen er "almenheten" eller særskilte NINA•NIKU, Tromsø grupper, f.eks. landbruket, fylkesmennenes miljøvern- avdelinger, turist- og friluftlivskretser o.l. -
Widespread and Accelerating Glacier Retreat on the Lyngen Peninsula, Northern Norway, Since Their ‘Little Ice Age’ Maximum
Journal of Glaciology (2018), 64(243) 100–118 doi: 10.1017/jog.2018.3 © The Author(s) 2018. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons. org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. Widespread and accelerating glacier retreat on the Lyngen Peninsula, northern Norway, since their ‘Little Ice Age’ maximum CHRIS R. STOKES,1 LISS M. ANDREASSEN,2 MATTHEW R. CHAMPION,1 GEOFFREY D. CORNER3 1Department of Geography, Durham University, Durham, DH1 3LE, UK 2Norwegian Water Resources and Energy Directorate (NVE), PO Box 5091 Majorstuen, N-0301 Oslo, Norway 3Department of Geosciences, UiT – The Arctic University of Norway, PO Box 6050 Langnes, N-9037 Tromsø, Norway Correspondence: Chris R. Stokes <[email protected]> ABSTRACT. The recession of mountain glaciers worldwide is increasing global sea level and, in many regions, human activities will have to adapt to changes in surface hydrology. Thus, it is important to provide up-to-date analyses of glacier change and the factors modulating their response to climate warming. Here we report changes in the extent of >120 glaciers on the Lyngen Peninsula, northern Norway, where glacier runoff is utilised for hydropower and where glacial lake outburst floods have occurred. Glaciers covered at least 114 km2 in 1953 and we compare this inventory with those from 1988, 2001 and a new one from 2014, and previously-dated Little Ice Age (LIA) limits. Results show a − steady reduction in area (∼0.3% a 1) between their LIA maximum (∼1915) and 1988, consistent with increasing summer air temperatures, but recession paused between 1988 and 2001, coinciding with increased winter precipitation. -
Tiltakssonen for Finnmark Og Nord-Troms - Utviklingstrekk Og Gjennomgang Av Virkemidlene
I samarbeid med Rapport 2012:2 Tiltakssonen for Finnmark og Nord-Troms - utviklingstrekk og gjennomgang av virkemidlene Elisabeth Angell (red), Sveinung Eikeland, Leo A.Grünfeld (Menon), Ivar Lie, Sindre Myhr, Vigdis Nygaard og Paul Pedersen Tittel: Tiltakssonen for Finnmark og Nord-Troms - utviklingstrekk og gjennomgang av virkemidlene Forfatter : Elisabeth Angell (red), Sveinung Eikeland, Leo A. Grünfeld, Ivar Lie, Sindre Myhr, Vigdis Nygaard og Paul Pedersen Norut Alta - Áltá rapport : 2012:2 ISBN : ISBN: 978-82-7571-214-9 Oppdragsgiver : Kommunal- og regionaldepartementet Prosjektleder : Elisabeth Angell Oppsummering : Utviklingstrekkene innen folketall har vært litt bedre i Tiltakssonen enn i andre periferiregioner, sysselsettingen har økt kraftig, særlig fra siste høykonjunktur fra 2005. Det har skjedd omstruktureringer i næringslivet med framveksten av petroleumsrelatert virksomhet, samtidig med en kraftig nedbygging av fiskeriene og fiskeindustrien. Fem næringsklynger er identifisert. Analyser av arbeidsgiveravgiften viser at en økt avgift påvirker sysselsettingen på kort sikt primært i tjenesteforetak, på lang sikt er virkningen uklar. De personrettede virkemidlene; skattelette, nedskriving av studielån og økt barnetrygd virker både rekrutterende og bostabiliserende for aldersgruppen 18-40 år, og særlig for de med høyere utdanning. Framover vil det også være behov for virkemidlene, særlig for å stimulere tilbudet av relevant arbeidskraft. Derfor foreslås det en kraftig styrking av de personrettede virkemidlene. Emneord : Regionalpolitikk, -
Planer Om Mer Vann Og Økt Produksjon I Skibotn Og Lavka Kraftverk I Storfjord Kommune
! ! Planer om mer vann og økt produksjon i Skibotn og Lavka kraftverk i Storfjord kommune Konsekvensvurdering på tema reiseliv ! ! ! Rapport MU2015-25 ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! !! Forsidebilde. På vei inn til Govdajavri fra Lavkadalen.! ! ! ! RAPPORT 2015-25 Prosjektansvarlig:! Utførende institusjon:! 34%!1%5.-.0*! #$%&'()*%$*!+,-./0$0*!12! Prosjektmedarbeider(e):! ! Oppdragsgiver:! Kontaktperson hos oppdragsgiver:! 6-789!:-)(,!3-7/;<9&70!12 =79,.$0!=.-<' Referanse:! 1%5.-.0*>!3?!@ABC?!3%)0.-!78!8.-!5)00!7*!'<,!D-7/;<9&70!$!2<$E7,0!7*!F)5<)!<-)(,5.-<!$!2,7-G (&7-/!<788;0.?!:709.<5.09;,-./0$0*!D4!,.8)!-.$9.%$5?!#$%&'()*%$*!+,-./0$0*!-)DD7-,!@ABCG@C>! H2IJ!KLMGM@GMB"MGLLNGM?! Referat:! #$%&'()*%$*!+,-./0$0*!12!O)-!;,)-E.$/.,!.0!,.8),$9<!<709.<5.09;,-./0$0*!$!(7-E$0/.%9.!8./! 6-789!:-)(,!3-7/;<9&70!12!9$0.!D%)0.-!78!,-.!;,5$<%$0*9D-79&.<,.-!$!2,7-(&7-/!<788;0.>!6-789! (P%<.?!6.8).,!978!<709.<5.09;,-./.9!$!/.00.!-)DD7-,.0!.-!-.$9.%$5?! Q75/)75.-('-$0*.0!7D.-.-.-!8./!,7!)%,.-0),$5.!;,EP**$0*9%'90$0*.->!Q75/)!"!7*!Q75/)!B>!978! ,)-!$00!O.0O7%/95$9!"!7*!B!9$/.E.<<!,$%!Q75/)&7O<)!$!07-/'9,9$/)!)5!'5-.!/.%.-!)5!I-.$//)%.0?! :709.<5.09.0.!.-!5;-/.-,!978!%$,.!0.*),$5.!(7-!E.**.!)%,.-0),$5.0.?!#.9,!;,9%)*9*$5.0/.!(7-! 9)8%.,!<709.<5.09!.-!R%$,.0S!0.*),$5!D45$-<0$0*!D4!($9<.-.99;-9.0.!7*!/.-5./!($9<.!978!-.$9.%$5G 9),,-)<9&70!$!2$*0)%/)%9.%5)?! T$.997*)9!.-!$!)%%!O75./9)<!%7<)%$9.-,!$00.0(7-!)%%.-./.!$00*-.D9E.-'-,!78-4/.>!8.0!,$%,)<.,! -.D-.9.0,.-.-!0P.!$00*-.D9(7-8.-?!:709.<5.09.0.!.-!5;-/.-,!978!984U8$//.%9!0.*),$5.?!#.9,! ;,9%)*9*$5.0/.!(7-!9)8%.,!<709.<5.09!.-!E7-,()%%.,!)5!(799.0!$!T$.997*)9&7O<)>!9)8,!0.*),$5!